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dc.contributor.authorPICKFORD, Martinen
dc.contributor.authorNAKAYA, Hideoen
dc.contributor.authorISHIDA, Hidemien
dc.contributor.authorNAKANO, Yoshihikoen
dc.date.accessioned2008-11-25T02:46:23Z-
dc.date.available2008-11-25T02:46:23Z-
dc.date.issued1984-03-
dc.identifier.issn0286-9667-
dc.identifier.urihttp://hdl.handle.net/2433/68315-
dc.description.abstractTo examine and refine the preliminary K-Ar dating results, the faunas of Nachola and Samburu Hills are analyzed biostratigraphically. It is confirmed that the fauna of Nachola is in the pre-Hipparion stage (earlier than 10±0.5 m.y.). The fauna from the Namurungule Formation of Samburu Hills is the post-Hipparion stage (later than 10±0.5), not as advanced as that of Lukeino (6.5 m.y.) and most like those from Ngeringerowa and Nakali. Therefore, it is supposed that the age of the Namurungule fauna is 9±1 m.y..en
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherThe Research Committee for African Area Studies, Kyoto Universityen
dc.subject.ndc240-
dc.titleThe Biostratigraphic Analyses of the Faunas of the Nachola Area and Samburu Hills, Northern Kenyaen
dc.typejournal article-
dc.type.niitypeJournal Article-
dc.identifier.ncidAA10636379-
dc.identifier.jtitleAfrican Study Monographs. Supplementary Issue.en
dc.identifier.volume2-
dc.identifier.spage67-
dc.identifier.epage72-
dc.textversionpublisher-
dc.sortkey05-
dc.addressNational Museums of Kenyaen
dc.addressFaculty of Science, Kyoto Universityen
dc.addressFaculty of Human Sciences, Osaka Universityen
dc.addressFaculty of Human Sciences, Osaka Universityen
dc.identifier.selfDOI10.14989/68315-
dcterms.accessRightsopen access-
dc.identifier.pissn0286-9667-
出現コレクション:2 (Study of the Tertiary Hominoids and Their Palaeoenvironments in East Africa: 2)

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